Climate and vegetation and their impact on stable C and N isotope ratios in bat guano

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dc.contributor.authorReid, Rachel E. B.en
dc.contributor.authorWaples, James T.en
dc.contributor.authorJensen, David A.en
dc.contributor.authorEdwards, Christine E.en
dc.contributor.authorLiu, Xinyien
dc.date.accessioned2023-05-09T12:43:03Zen
dc.date.available2023-05-09T12:43:03Zen
dc.date.issued2022-09en
dc.description.abstractCave guano deposits represent a relatively untapped paleoecological archive that can provide information about past vegetation, climate, and bat diet over several millennia. Recent research suggests that carbon isotope values (delta C-13) measured in guano accumulations from insectivorous bats reflect the relative abundance of C-3 and C-4 plants on the landscape while nitrogen isotope values (delta N-15) may reflect precipitation amount. Together, these proxies can provide useful information for restoration practitioners seeking to understand how plant species composition has changed over time in relation to climate and land use. To better calibrate these proxies for use in restoration, we compared instrumental records of precipitation and satellite imagery of vegetation with isotope values measured in modern bat guano from Mary Lawson Cave, a large limestone cavern located in central Missouri. Mary Lawson Cave hosts a maternity colony of insectivorous gray bats (Myotis grisescens), and as such, contains significant guano accumulations. In the fall of 2018, we collected a 60 cm long guano core that dates to 1999 cal AD at its base. Guano core delta C-13 values decrease from the base toward the surface (from similar to-26 to -27 parts per thousand) whereas delta N-15 values increase toward the surface even after accounting for ammonia volatilization (from similar to 3 to 5 parts per thousand). Presently, the landscape around Mary Lawson Cave is dominated by a deciduous forest and pasture. Given that the land cover has changed very little over this period, the decline in delta C-13 values toward the present likely reflects a shift in land management on farms and/or increases in invasive C-3 species. Rainfall amounts from nearby Lebanon, Missouri, are significantly positively correlated with guano delta N-15 values, a relationship that is notably opposite that observed previously in soil and plants. We argue that heavy fertilizer application and significant grazing intensity could lead to the accumulation of large pools of excess labile nitrogen which would be vulnerable to leaching during precipitation events. The relationship between guano delta N-15 values and precipitation may differ for materials from less agriculturally impacted locations or periods and should be extended into the past with caution.en
dc.description.notesFunding The funding for this research was provided by the Living Earth Collaborative and the International Center for Energy, Environment and Sustainability. The Virginia Tech Open Access Subvention Fund provided funding to support the publication of this article.en
dc.description.sponsorshipVirginia Tech Open Accessen
dc.description.versionPublished versionen
dc.format.mimetypeapplication/pdfen
dc.identifier.doihttps://doi.org/10.3389/fevo.2022.929220en
dc.identifier.other929220en
dc.identifier.urihttp://hdl.handle.net/10919/114986en
dc.identifier.volume10en
dc.language.isoenen
dc.publisherFrontiersen
dc.rightsCreative Commons Attribution 4.0 Internationalen
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/en
dc.subjectguanoen
dc.subjectcarbonen
dc.subjectnitrogenen
dc.subjecttime seriesen
dc.subjectprecipitationen
dc.subjectvegetationen
dc.subjectrestorationen
dc.titleClimate and vegetation and their impact on stable C and N isotope ratios in bat guanoen
dc.title.serialFrontiers in Ecology and Evolutionen
dc.typeArticle - Refereeden
dc.type.dcmitypeTexten

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